Sulfidic organic-rich shales in the Archean low-sulfate ocean: Evidence for transient oxygenated conditions, enhanced volcanism, or low sedimentation rates?

Details Sulfidic organic-rich shales in the Archean low-sulfate ocean: Evidence for transient oxygenated conditions, enhanced volcanism, or low sedimentation rates? Sulfidic organic-rich shales in the Archean low-sulfate ocean: Evidence for transient oxygenated conditions, enhanced volcanism, or low sedimentation rates?

Jul 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008gecas..72q..69b&link_type=openurl

Geochimica et Cosmochimica Acta, Volume 72, Issue 12, p.A69

Physics

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